We measured the distribution of particulate and dissolved pools of the phytoplankton osmolyte dimethylsulfoniopropionate (DMSP) in the euphotic zone at a series of shelf (Ͻ40 m total water depth) and oceanic (Ͼ500 m depth) stations in the northern Gulf of Mexico. We also measured turnover rates of the dissolved DMSP pools (DMSPd) with tracer additions of 35 S-DMSPd and short-term (Ͻ1 h) incubations, with the aim of examining the relationship between DMSPd turnover and bacterial production. Particulate DMSP concentrations were relatively low (Ͻ25 nM) throughout the study area with about twofold higher mean concentration at the shelf sites (15 nM) compared with the oligotrophic oceanic sites (7 nM). DMSPd concentrations averaged 3.0 nM in shelf waters and 1.3 nM in oceanic waters. Concentrations of dimethylsulfide (DMS), a degradation product of DMSP, also were low throughout the Gulf, averaging 2.0 nM for all depths sampled and 2.5 nM in surface waters. Microbial assemblages metabolized 35 S-DMSPd with the sulfur being incorporated into biomass, volatile compounds (DMS and methanethiol), and other dissolved products. DMSPd turnover was relatively slow (mean of 3.8 nM d
Ϫ1) in oligotrophic oceanic waters and averaged 10-fold higher (39 nM d
Ϫ1) in mesotrophic shelf waters. DMS concentrations ranged from 0.2 to 5.1 nM in oceanic waters and appeared to be weakly related to DMSP turnover. In contrast, DMS concentrations in shelf waters fell within a narrow range (0.8-2.8 nM) and showed no relationship at all with DMSPd turnover. DMSPd turnover rates were high enough to sustain the measured concentrations and estimated turnover of DMS, even if the conversion efficiency of DMSPd into DMS was only 10%. DMSPd turnover was significantly correlated with bacterial production (as measured by 3 H-thymidine incorporation) and we estimate that DMSPd turnover contributed a mean of 3.4% of the carbon and ϳ100% of the sulfur required for bacterial growth in Gulf of Mexico surface waters. In addition to its role as a precursor of DMS, DMSP deserves attention as an important substrate for bacterioplankton in the euphotic zone.Dimethylsulfoniopropionate ((CH 3 ) 2 S ϩ CH 2 CH 2 COO Ϫ ; DMSP) is a sulfur-containing compound that is produced by a wide variety of marine phytoplankton and is distributed throughout the euphotic zone of the oceans (Keller et al. 1989;Kettle et al. 1999). DMSP is present in operationallydefined particulate (DMSPp) and dissolved (DMSPd) forms with the DMSPp pool consisting of filterable phytoplankton and organisms that have accumulated DMSP from their diet. Concentrations of DMSPp typically range from 5 to Ͼ300 nM depending on factors such as phytoplankton biomass and species composition (Iverson et al. 1989;Malin et al. 1993). The dissolved DMSP pool is generally smaller (1-50 nM) than the particulate pool, but is believed to be more dynamic, with turnover times estimated to be on the order of hours in subtropical waters (Kiene 1996b;Ledyard and Dacey 1996). 1 Corresponding author (rkiene@jaguar1.u...